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Article Navigation >  Acta Sedimentologica Sinica  > 1986  >  4(2): 69-80

Cui Zhijiu. PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT[J]. Acta Sedimentologica Sinica, 1986, 4(2): 69-80.
Citation: Cui Zhijiu. PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT[J]. Acta Sedimentologica Sinica, 1986, 4(2): 69-80.
shu

PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT

  • Department of Geography, Peking University

  • Received Date: 1984-05-22
  • Publish Date: 1986-06-10
  • In this paper, such terrigenous elastic deposit, which has a large disparity in gram size with no sorting or a little sorting, and coarse elastic particles scattered in fine filling matrixes, 0r fine particles filled amoag interstice of coarse clastics, is defined as diamicton or diamictite.Debris flow deposit is one of the diamictons. Over a long time, it has encountered a lot of difficulties to distinguish the genesis of diamicton at home and abroad.
  • [1] 钱宁等，1984，地理学报，39卷，1期，20-33页。
    [2] 吴积善，1981，泥石流体的结构，泥石流论文集(1 )，科学技术文献出版社重庆分社，38-66页。
    [3] 中国科学院兰州冰川冻土研究所，甘肃省交通科学研究所，1982，甘肃泥石流，人民交通出版社。
    [4] 姚德基等，1981，国外泥石流研究中的若干基本理论问题，泥石流论文集(1)，科学技术文献出版社重庆分社，142-150页。
    [5] Enos, P.1977, Sedimentology., 24( 1)，133-142.
    [6] Lowe, D.R.1976, J, Sedim, Petrol., Vol, 46, No, 1, 188-199.
    [7] Fairbridge, R.W., Bourgeois, J., 1978, E ncyclopedia of E arth Sciences Se-ries, Vol.6, The Encyclopedia of Sedimentology.
    [8] Bull, W.B.1963, J. of G eology., V o1.71, 243 -251.
    [9] Gascoyen, P., 1978, E ncyclopedia of Sedimentology, 488-493
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  • Received:  1984-05-22
  • Published:  1986-06-10

PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT

  • Department of Geography, Peking University
  • Received Date: 1984-05-22
  • Publish Date: 1986-06-10

Abstract: In this paper, such terrigenous elastic deposit, which has a large disparity in gram size with no sorting or a little sorting, and coarse elastic particles scattered in fine filling matrixes, 0r fine particles filled amoag interstice of coarse clastics, is defined as diamicton or diamictite.Debris flow deposit is one of the diamictons. Over a long time, it has encountered a lot of difficulties to distinguish the genesis of diamicton at home and abroad.

Cui Zhijiu. PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT[J]. Acta Sedimentologica Sinica, 1986, 4(2): 69-80.
Citation: Cui Zhijiu. PRELIMINARY STUDY ON TYPES, MACROSCOPIC CHARACTERISTICS AND GENESIS-MECHANISM OF DEBRIS FLOW DEPOSIT[J]. Acta Sedimentologica Sinica, 1986, 4(2): 69-80.
shu

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